In the last lesson we made one fixed tone. The thing that makes one tone different from another - high versus low, squeaky versus rumbly - is frequency.
Frequency = how many times the wave completes a full cycle in one second. One cycle = one hill and one valley. We measure it in Hertz (Hz). One Hertz means one cycle per second.
Drag the slider. Watch the oscilloscope. As frequency goes up, the wave gets squished together - more cycles crammed into the same space. As frequency goes down, the wave stretches out lazily. Same shape, different speed.
Both waves have the same amplitude (same volume). The only difference is how many cycles fit in the same time span. More cycles = higher pitch.
Human hearing runs from roughly 20 Hz (a bass so low it is more felt than heard) to 20,000 Hz (a piercing whistle that fades as you age). Most adults cannot hear above 15,000 Hz.
This machine goes up to 10,000 Hz. Above that, sine waves just become irritating.
Try the octave buttons. An octave is what happens when you double the frequency. C4 is 261.63 Hz. C5 is 523.25 Hz - exactly double.
Your brain perceives doubled frequencies as "the same note, but higher." This is not a cultural convention. It is baked into auditory neuroscience across every human culture ever studied, and several animal species too.
The note buttons give you C4 through C5, plus A4 at 440 Hz - the reference pitch that orchestras tune to. When someone says "concert pitch" or "A440," they mean this exact frequency.
It was standardised in 1955 by the International Organisation for Standardisation, which is exactly the sort of committee you would expect to have opinions about the precise frequency of a musical note.
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